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Summerschool Design our future with data https://www.kennislabvoorurbanisme.nl/project/summerschool-aug-2019/
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The water budget
The water budget, or water balance, of a drainage basin shows the relationship between precipitation, evapotranspiration, surface runoff, and changes in water storage. It is often expressed as an equation where precipitation equals surface runoff plus evapotranspiration plus or minus changes in storage. The water budget is useful for hydrologists to understand water surplus and deficit, and to plan for potential water shortages or recharge after deficit. A water budget graph illustrates surplus when precipitation exceeds evapotranspiration and deficit when the reverse is true.
HYDRAULICAL BUDGET AND CATCHMENT AREA
The hydrological budget equation describes the flow of water in and out of a system. It accounts for all water inflows such as precipitation and outflows like evaporation, transpiration, runoff, and groundwater flow. The difference between total inflows and outflows is equal to the change in water storage. The hydrological budget is used to analyze water availability and flows within a catchment area, which is defined as the region where surface water converges to a single point like a lake or river.
Water Balance VLE
The water balance, or budget, is a simple equation used to understand water resources in a drainage basin. It accounts for precipitation, evapotranspiration, infiltration into soils, storage of water in soils, and outputs like surface runoff and flow into rivers. When precipitation exceeds evapotranspiration, soils become saturated and excess water runs off as overland flow, contributing to rivers. When evapotranspiration is greater than precipitation, stored soil moisture is reduced and depleted.
WFP Hydrologic cycle
The document discusses the most important factors for a water harvesting system. It lists climate, hydrology, topography, agronomy, soils, and socio-economics as the key factors. Hydrology is defined as dealing with the full life cycle of water on Earth, including its occurrence, circulation, distribution, properties, and interaction with the environment.
Water balance calculation
This document presents an overview of water balance calculations. It defines water balance and its components such as precipitation, evapotranspiration, soil moisture, surplus and deficit. It describes different types of water balances including surface water, groundwater, soil water, lake water and oceanic water balances. The document discusses applications of water balance calculations and limitations. It concludes that water balance estimation is an important tool for assessing water resources and supporting water management decisions.
Chapter 2 hydrologic cycle
1. The document discusses key concepts in hydrology including the hydrologic cycle, water budget equation, and groundwater components.
2. The hydrologic cycle describes the continuous movement of water on, above, and below the surface of the Earth, including evaporation, transpiration, precipitation, and subsurface flow.
3. The water budget equation expresses the principle of conservation of mass by equating water inputs such as precipitation to outputs like evapotranspiration and changes in storage over a given time period for a defined catchment area.
Drainage basins and water budgets
The document discusses key concepts related to the hydrological cycle including drainage basins, stream ordering, drainage density, and water budgets. It prompts students to explain these concepts using terms like evapotranspiration, soil moisture utilization, soil moisture recharge, positive and negative water budgets, and field capacity. Students are also asked to consider if the UK and Greece have an overall positive or negative water budget and to review textbook pages in preparation for the next lesson.
Surface Runoff Full Presentatiom
Surface runoff occurs when rainwater pools on the surface after infiltrating the soil to its maximum capacity. It flows across the land into low points and bodies of water, carrying pollutants from urban and agricultural areas that can harm the environment, wildlife, and water quality. Increased urbanization reduces groundwater recharge and exacerbates drought by preventing water absorption, impacting farmers and communities that rely on well water. Contaminants transported by surface runoff threaten aquatic species through fish kills, population imbalances, and interference with reproduction. Simple actions like proper pesticide use, cleaning up pet waste, and recycling motor oil can help reduce pollutants entering watersheds via surface runoff.
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The water budget
The water budget, or water balance, of a drainage basin shows the relationship between precipitation, evapotranspiration, surface runoff, and changes in water storage. It is often expressed as an equation where precipitation equals surface runoff plus evapotranspiration plus or minus changes in storage. The water budget is useful for hydrologists to understand water surplus and deficit, and to plan for potential water shortages or recharge after deficit. A water budget graph illustrates surplus when precipitation exceeds evapotranspiration and deficit when the reverse is true.
HYDRAULICAL BUDGET AND CATCHMENT AREA
The hydrological budget equation describes the flow of water in and out of a system. It accounts for all water inflows such as precipitation and outflows like evaporation, transpiration, runoff, and groundwater flow. The difference between total inflows and outflows is equal to the change in water storage. The hydrological budget is used to analyze water availability and flows within a catchment area, which is defined as the region where surface water converges to a single point like a lake or river.
Water Balance VLE
The water balance, or budget, is a simple equation used to understand water resources in a drainage basin. It accounts for precipitation, evapotranspiration, infiltration into soils, storage of water in soils, and outputs like surface runoff and flow into rivers. When precipitation exceeds evapotranspiration, soils become saturated and excess water runs off as overland flow, contributing to rivers. When evapotranspiration is greater than precipitation, stored soil moisture is reduced and depleted.
WFP Hydrologic cycle
The document discusses the most important factors for a water harvesting system. It lists climate, hydrology, topography, agronomy, soils, and socio-economics as the key factors. Hydrology is defined as dealing with the full life cycle of water on Earth, including its occurrence, circulation, distribution, properties, and interaction with the environment.
Water balance calculation
This document presents an overview of water balance calculations. It defines water balance and its components such as precipitation, evapotranspiration, soil moisture, surplus and deficit. It describes different types of water balances including surface water, groundwater, soil water, lake water and oceanic water balances. The document discusses applications of water balance calculations and limitations. It concludes that water balance estimation is an important tool for assessing water resources and supporting water management decisions.
Chapter 2 hydrologic cycle
1. The document discusses key concepts in hydrology including the hydrologic cycle, water budget equation, and groundwater components.
2. The hydrologic cycle describes the continuous movement of water on, above, and below the surface of the Earth, including evaporation, transpiration, precipitation, and subsurface flow.
3. The water budget equation expresses the principle of conservation of mass by equating water inputs such as precipitation to outputs like evapotranspiration and changes in storage over a given time period for a defined catchment area.
Drainage basins and water budgets
The document discusses key concepts related to the hydrological cycle including drainage basins, stream ordering, drainage density, and water budgets. It prompts students to explain these concepts using terms like evapotranspiration, soil moisture utilization, soil moisture recharge, positive and negative water budgets, and field capacity. Students are also asked to consider if the UK and Greece have an overall positive or negative water budget and to review textbook pages in preparation for the next lesson.
Surface Runoff Full Presentatiom
Surface runoff occurs when rainwater pools on the surface after infiltrating the soil to its maximum capacity. It flows across the land into low points and bodies of water, carrying pollutants from urban and agricultural areas that can harm the environment, wildlife, and water quality. Increased urbanization reduces groundwater recharge and exacerbates drought by preventing water absorption, impacting farmers and communities that rely on well water. Contaminants transported by surface runoff threaten aquatic species through fish kills, population imbalances, and interference with reproduction. Simple actions like proper pesticide use, cleaning up pet waste, and recycling motor oil can help reduce pollutants entering watersheds via surface runoff.
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The document discusses the growing problem of plastic pollution in the world's oceans. It references a quote from Jacques-Yves Cousteau about water and air becoming "global garbage cans" due to increasing plastic debris. It then directs the reader to map global surface ocean currents, trace how wind patterns impact currents, and compare real-time current data to reference maps showing typical ocean circulation patterns in order to better understand how plastic pollution is distributed worldwide by ocean transport.
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The document discusses engineering hydrology, which uses hydrologic principles to solve problems related to water resource management and development. It defines engineering hydrology as studying the hydrologic cycle and its components like precipitation, evaporation, infiltration and runoff. Engineering hydrologists work on projects for water control, utilization and management by estimating maximum floods, droughts, water supply and more using statistical and modeling techniques. The key aspects of hydrology discussed are data collection, analysis and prediction.
Hydrosphere
The hydrosphere describes all water on, under, and over the surface of a planet. The water cycle describes the continuous movement of water through different states and reservoirs on Earth through processes like evaporation and condensation. Surface runoff occurs when rain or snowmelt causes water to flow over the land rather than being absorbed by the soil.
Water resources situation in Greece
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The hydrologic cycle and water resource of world
The hydrologic cycle describes the continuous movement of water on, above, and below the surface of the Earth. Water is evaporated from oceans and land surfaces, rises into the atmosphere, cools and condenses to form clouds, and falls again as precipitation. Some precipitation runs off surfaces and becomes surface water in oceans, seas, rivers, lakes, and groundwater; other precipitation is intercepted by trees and vegetation; and some infiltrates and recharges groundwater stores. Water is also transpired into the atmosphere from plants and other surfaces. The hydrologic cycle involves the balanced circulation of water in the hydrosphere, atmosphere, geosphere, and biosphere.
Water balance
The document discusses the water balance of a drainage basin. It is made up of precipitation inputs, evapotranspiration outputs, and storage changes. Precipitation is the primary water input. Evapotranspiration is water released into the air by evaporation from wet surfaces and transpiration from plants. The water balance equation expresses that precipitation equals total streamflow discharge plus evapotranspiration, plus or minus changes in water storage.
Water cycle and water budget
This document provides information about the hydrological cycle and water budget. It begins with the objectives of understanding water sources and the hydrological cycle components of evaporation, precipitation, infiltration, runoff and subsurface flow. It then discusses the global water resources and usage, including increasing population growth. The bulk of the document defines and explains the various components of the hydrological cycle, including evaporation, condensation, precipitation types, interception, infiltration, subsurface flow, runoff and storage. It provides an example water balance equation and long-term water balance calculation. Finally, it briefly discusses the global water cycle and a typical hydrological cycle for the UAE.
Hydrologic Cycle
Water is essential for life and the hydrologic cycle distributes it around the planet. The cycle involves evaporation, transpiration, condensation, precipitation, collection as runoff or infiltration into groundwater, and storage in oceans, glaciers, and ice caps. Climate is influenced by the hydrologic cycle as warm air holds more water vapor and rising air cools, causing precipitation. Changes to the cycle, such as intensification due to climate change, can produce more extreme flooding and drought.
Evapotranspiration
This document discusses evapotranspiration (ET), which is the combination of evaporation from soil and transpiration from crops. ET depends on factors like solar radiation, temperature, humidity, wind speed, soil water availability, and crop development. Early in the growing season when crops are small, most water loss is from soil evaporation, but as crops develop and their canopies shade more of the ground, transpiration becomes the dominant process of ET. The rate of ET is typically expressed in millimeters of water lost per time period, like 1 mm per day.
Practical Applications of Hydrology
This document discusses practical applications of hydrology. It begins by defining hydrology as the science of water on Earth, including its occurrence, movement, distribution, and circulation. Hydrology can be scientific or applied/engineering. Engineering hydrology deals with water resource estimation, precipitation/runoff processes, and flood/drought problems. Some key practical applications of hydrology include water supply and treatment, irrigation, drainage, hydropower, flood control, and pollution control. Hydrology and hydraulics intersect in areas like water supply, power generation, dams/reservoirs, flood protection, and wastewater management. Engineering uses of surface water hydrology include modeling average and extreme events for applications like infrastructure design, water supply
Hydrological cycle and its components
The document discusses the hydrological cycle and its components. The hydrological cycle describes the storage and movement of water between the biosphere, atmosphere, lithosphere, and hydrosphere. Water evaporates from oceans and transpiration from plants, condenses to form clouds, and precipitates as rain or snow. Precipitation runs off and infiltrates the ground, becoming groundwater that eventually discharges into water bodies, completing the cycle as water evaporates again from oceans. The main components are evaporation, transpiration, condensation, precipitation, runoff, infiltration, and groundwater flow.
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Presentation showing the workings of the Hydrological cycle for AS level students
The Hydrologic Cycle
The document provides an overview of the hydrologic cycle. It begins with an introduction explaining that water circulates continuously between different spheres of the Earth. It then discusses the major components of the hydrologic cycle, including precipitation, evaporation, transpiration, runoff, infiltration, and others. Finally, it explains concepts like condensation and how precipitation forms from water vapor in the atmosphere. The overall document serves to describe the world's water circulation and the relationships between different elements of the hydrologic cycle.
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UNESCO is contributing to advancing knowledge on groundwater resources in the Arab region through two programs: GWG and TWAP. GWG aims to improve groundwater governance, holding regional consultations to identify needs. Main needs identified were improving data, strengthening water institutions, increasing transparency, and communication/awareness efforts. TWAP conducts global assessments of transboundary waters using a methodology addressing hydrogeological, environmental, socioeconomic and legal/institutional factors. The goal is to promote financing for improved management of transboundary systems through stakeholder engagement.
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The document discusses the water balance of a drainage basin. It is made up of precipitation inputs, evapotranspiration outputs, and storage changes. Precipitation is the primary water input. Evapotranspiration is water released into the air by evaporation from wet surfaces and transpiration from plants. The water balance equation expresses that precipitation equals total streamflow discharge plus evapotranspiration, plus or minus changes in water storage.
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This document provides information about the hydrological cycle and water budget. It begins with the objectives of understanding water sources and the hydrological cycle components of evaporation, precipitation, infiltration, runoff and subsurface flow. It then discusses the global water resources and usage, including increasing population growth. The bulk of the document defines and explains the various components of the hydrological cycle, including evaporation, condensation, precipitation types, interception, infiltration, subsurface flow, runoff and storage. It provides an example water balance equation and long-term water balance calculation. Finally, it briefly discusses the global water cycle and a typical hydrological cycle for the UAE.
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Water is essential for life and the hydrologic cycle distributes it around the planet. The cycle involves evaporation, transpiration, condensation, precipitation, collection as runoff or infiltration into groundwater, and storage in oceans, glaciers, and ice caps. Climate is influenced by the hydrologic cycle as warm air holds more water vapor and rising air cools, causing precipitation. Changes to the cycle, such as intensification due to climate change, can produce more extreme flooding and drought.
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Summerschool ‘Wie maakt de slimme stad leuk?’ op 23, 24 en 25 augustus 2021 in Den Haag.
Product team 4
Summerschool ‘Wie maakt de slimme stad leuk?’ op 23, 24 en 25 augustus 2021 in Den Haag.
Presentatie team 3
Summerschool ‘Wie maakt de slimme stad leuk?’ op 23, 24 en 25 augustus 2021 in Den Haag.
Product team 3
Summerschool ‘Wie maakt de slimme stad leuk?’ op 23, 24 en 25 augustus 2021 in Den Haag.
Team 1 presentatie
Summerschool ‘Wie maakt de slimme stad leuk?’ op 23, 24 en 25 augustus 2021 in Den Haag.
Team 5 - presentatie - Identituin
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 5 - product - Identituin
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 4 - presentatie - Tuinwerken
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 3 - presentatie - Ik wil een boom
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 2 - presentatie- Vlinderpunten
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 1 - product - Handje groen, tuintje groen
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
Team 1 - Handje groen, tuintje groen
Summerschool 'Ontwerp de nieuwe norm voor de groene tuin'
https://www.kennislabvoorurbanisme.nl/project/summerschool-okt-2020/
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Team 2 - presentatie - Summerschool 'Maak je eigen slimme stad'
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Presentatie team 5
- 1. A D L P
- 2. Why could this be our Future? “The soil subsidises faster than the sea-level will rise” Source, Platform slappe bodem (n.d.)
- 5. What is the relevance of this challenge 22 Billion - Affects on flora and fauna - Changing landscapes Source; PBL (2016)
- 6. Time-line prediction of salinization
- 8. Identity and cultural value of the Zuid-Holland landscape
- 10. For example: Economic value Keukenhof Keukenhof (2017) Visitors 1,4 million Dutch visitors 20% Foreign visitors 80% Revenues (in million euros) 23,8
- 11. Policy implication Short term actions for Long term effects
- 12. 4 strategies in tackling saline • Active rewetting • Passive rewetting
- 14. • Deep water drainage
- 15. Introducing a 5th strategy • Salt filtering vegitation
- 18. Measuring and monitoring Water quality and cloride levels → expanding dataset